May 2008 Earthquake in China Could Be Followed by Another Significant Rupture

Researchers analyzing the May 2008 Wenchuan earthquake in China’s Sichuan
province have found that geological stress has significantly increased on three
major fault systems in the region. The magnitude 7.9 quake on May 12 has
brought several nearby faults closer to failure and could trigger another major
earthquake in the region.

Geophysicists used computer models to calculate the changes
in stress along the Xianshuihe, Kunlun, and Min Jiang faults—strike-slip faults
like the San Andreas—which lie about 150 to 450 kilometers (90 to 280 miles)
from the Longmen Shan rupture that caused the devastating quake. The research
team also examined seismic activity in the region over the past decade.

They found that the May 12 event has doubled the
probabilities of future earthquakes on these fault lines. Specifically, they
estimated the probability of another earthquake of magnitude 6 or greater in
the region is 57 to 71 percent over the next decade.
There is an 8 to 12 percent chance of a quake larger than magnitude 7 in the
next decade and 23-31 percent in the next 30 years.

The research team was led by Shinji Toda of the Geological
Survey of Japan, and includes Jian Lin of the Woods Hole Oceanographic
Institution (WHOI), Mustapha Meghraoui of the Institute of Geophysics in
Strasbourg (France), and Ross Stein of the U.S. Geological Survey (USGS). Their
findings were published September 9 in the online edition of the journal Geophysical Research Letters.

“One great earthquake seems to make the next one more
likely, not less,” said Stein, who has been collaborating with Lin and Toda for
nearly two decades. “We tend to think of earthquakes as relieving stress on a
fault. That may be true for the one that ruptured, but not for the adjacent
faults.”

In 1999, a 7.4 magnitude earthquake in Izmit, Turkey,
was followed four months later by an M7.1 event in nearby Duzce. The
devastating December 2004 Sumatra earthquake
(M9.2) and tsunami were followed by an M8.7 quake three months later.

“Because the Tibetan Plateau is one of the most seismically
active regions in the world, we believe there is credible evidence for a new
major quake in this region,” said Lin, a senior scientist in WHOI’s Department
of Geology and Geophysics. “The research community cannot forecast the timing
of earthquakes, and there are still significant uncertainties in our models.
But the Turkey and Sumatra events indicate that one major earthquake can
indeed promote another.

Researchers see it as a domino-like effect, where the
movement of one piece of Earth’s crust means that another piece must move up,
down, or away. While the stress in the crust gets reduced in some locations, it
is transferred to other faults nearby.

Large aftershocks that occurred on August 1 and 5 in the Sichuan region of China may fit with this predicted
pattern.

“Earthquake prediction is a bit like the thundercloud and
lightning,” Toda explained. “We can forecast that lightning will come from a
thundercloud, but we cannot predict the exact time and place where the
lightning will hit. With earthquakes, we can roughly forecast the probability
of activity over broad ranges of time, magnitude, and location, but we cannot
determine the exact value for any of these.”

On May 12, 2008, about 300 kilometers of the Longmen Shan
fault zone ruptured in an earthquake that killed at least 69,000 people and
left another 5 million homeless. It was the deadliest and strongest earthquake
to hit China since the 1976 Tangshan earthquake,
which killed at least 240,000.

As pieces of the Longman Shan fault slipped by as much as
nine meters (28 feet) in the May quake, stress increased along the neighboring
Xianshuihe, Kunlun, and Min Jiang faults, according to Toda and colleagues. All
three faults have a history of large quakes, though portions of each have been
quiet for most of the past century. All three faults were considered to be
primed for an earthquake even before the recent events.

In addition to the broad prediction of earthquake
triggering, the researchers have also forecasted the rate and distribution of
seismic shocks greater than magnitude 6, a prediction that they plan to test
from seismic stations over the next decade.

“Our paper predicts the change in the rate of small
earthquakes for the faults in the region, and now we can test that prediction,”
said Stein. “If the rate of shocks increases on the adjacent faults, then we
can confirm at least part of our hypothesis that large shocks are also more
likely. It may take time, but it is a testable hypothesis.”

In western China,
the intrusion of the Indian sub-continent pushes the Tibetan Plateau up and
over the older Sichuan
Basin and other parts of
the Eurasian continent. An estimated 33 percent of world’s continental
earthquakes occur in China,
even though it only occupies 7 percent of the planet’s land mass. Nearly 55
percent of all human loss to earthquakes occurs in China.

“Earthquakes do not kill people, buildings do,” said Lin,
who was a high school student in China
when the devastating Tangshan
earthquake struck. “There needs to be widespread education in earthquake
preparedness, as well as systematic inspection of buildings in these regions of
heightened risk. Every new building inspection and evacuation plan could
potentially save lives.”

“We hope the long-term forecasting allows the Chinese
government to make it a priority to mitigate future damage,” Toda added. “We
recommend that Chinese scientists carefully observe changes in seismicity by
installing new seismometers in the region."

Lin, Toda, and Stein were preparing to teach an earthquake
modeling course to Meghraoui’s students and colleagues in France when the
May 12 earthquake occurred. The researchers immediately went into action,
working with an international group of scientists to analyze the new stresses
on the system.

An early version of the manuscript by Toda et al was circulated to several dozen
Chinese scientists and government officials as they sought to assess the risk
of aftershocks in the weeks after the earthquake. Chinese government
organizations and scientists are now examining the paper in detail.

“The recent quake reminded us that Earth scientists have a
tremendous responsibility to work on issues of societal relevance,” said Lin.
“We don’t want to create panic, but there is legitimate cause for concern and
we have a major role to play in educating the public about what we know.”

Funding for this research was provided by the Charles D. Hollister Endowed Fund for Support of
Innovative Research at WHOI and the
EOST-Institut de Physique du Globe de Strasbourg, France.

Through computer modeling, researchers have
calculated the shifting and changes in stress within earth's crust in
the regions adjoining the May 2008 Wenchuan earthquake. Yellows and
reds indicate areas of heightened stress, which are clustered around
three faults that have produced large earthquakes within the past
century. The yellow star indicates the main shock on May 12, with the
black dots representing the aftershocks from May 12-20.
(Toda, Lin, Meghraoui, and Stein, reprinted from Geophysical Research Letters)

In order to test the validity of their earthquake prediction, Toda et
al plotted seismic activity in the decade leading up to the May 2008
earthquake and forecasted the rate of activity for the next ten years. By issuing a forecast for even low-level activity, the research team hopes to observe how future events match up with their prediction.
(Toda, Lin, Meghraoui, and Stein, reprinted from Geophysical Research Letters)

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